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Fayil:Dobbingstone Burn - geograph.org.uk - 1291882.jpg

Dobbingstone_Burn_-_geograph.org.uk_-_1291882.jpg ‎(pikisal 640 × 426, girman fayil: 121 KB, irin MIME: image/jpeg)

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English: Dobbingstone Burn Looking downstream at the point where the burn enters a narrow part of its valley. This is a typical small burn cutting through relatively soft glacial deposits. The exposed sides show glacial till with all shapes and sizes of stones. The burn course is littered with huge boulders which have been released from the till.
Rana
Masomi From geograph.org.uk
Marubucin Mary and Angus Hogg
Jinginarwa
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Mary and Angus Hogg / Dobbingstone Burn / 
CC BY-SA 2.0
Mary and Angus Hogg / Dobbingstone Burn
Camera location55° 15′ 54″ N, 4° 40′ 11″ W  Heading=292° Kartographer map based on OpenStreetMap.View this and other nearby images on: OpenStreetMapinfo
Object location55° 15′ 55″ N, 4° 40′ 16″ W  Heading=292° Kartographer map based on OpenStreetMap.View this and other nearby images on: OpenStreetMapinfo

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This file is licensed under the Creative Commons Attribution-Share Alike 2.0 Generic license.
Jinginarwa: Mary and Angus Hogg
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Abubuwan da aka nuna a cikin wannan fayil

depicts Turanci

maƙirƙiri

Wasu muhimman ba tare da Wikidata kayayyaki ba

sunan mawallafi: Mary and Angus Hogg
URL Turanci: https://www.geograph.org.uk/profile/7257
object has role Turanci: mai daukar hoto

copyright status Turanci

copyrighted Turanci

farawa

2 Mayu 2009

coordinates of the point of view Turanci

55°15'54.50"N, 4°40'10.56"W

heading Turanci: 292 digiri

captured with Turanci

Nikon D50 Turanci

coordinates of depicted place Turanci

55°15'55.37"N, 4°40'15.60"W

heading Turanci: 292 digiri

exposure time Turanci

0.008 sakan

f-number Turanci

16

focal length Turanci

26 millimetre

media type Turanci

image/jpeg

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Rana/LokaciWadar sufaKusurwowiMa'aikaciBahasi
na yanzu09:19, 27 ga Faburairu, 2011Wadar sufa ta zubin 09:19, 27 ga Faburairu, 2011640 × 426 (121 KB)GeographBot== {{int:filedesc}} == {{Information |description={{en|1=Dobbingstone Burn Looking downstream at the point where the burn enters a narrow part of its valley. This is a typical small burn cutting through relatively soft glacial deposits. The exposed side

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